Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI42E13SW00022

Record: MDI42E13SW00022

General

Mineral Record Identification
Record Name(s) Greenoaks Mine - 1947
Related Record Type Partial
Related Record(s)
Record Status Developed Prospect Without Reported Reserves or Resources
Date Created 1987-Oct-23
Date Last Modified 2022-Mar-23
Created By
Revised By

Commodities

Primary Commodities: Gold

Secondary Commodities: Copper, Silver



Location

Township or Area: Pifher, Elmhirst

Latitude: 49° 48' 33.17"    Longitude: -87° 45' 56.92"

UTM Zone: 16    Easting: 444900   Northing: 5517700    UTM Datum: NAD83

Resident Geologist District: Thunder Bay North

NTS Grid: 42E13SW

Point Location Description: Minesite

Location Method: Conversion from MDI

Access Description: The property is located in Pifher and Elmhirst Townships. Travel north on Highway 801, which leaves Highway 11 approximately 23 km east of Beardmore, to the Namewaminikan (Sturgeon) River, a distance of 14 km. Continue north along Highway 801 for 6 km and turn east along a bush road, staying on the left fork, for about 1.5 km to the property.



Exploration History

1947: A.E. Rissanen discovered the Greenoaks Mine, consisting of the No 1, 2 3 and 4 zones. Stripping, trenching (No. 1, 2, 3 and 4 zones) and diamond drilling (22 holes totalling 448.7 m on the No. 1 zone) were completed. 1948: Greenoaks Mines Ltd. purchased 10 claims. 1953: Greenoaks purchased 5 remaining claims. Resistivity, mag and geological surveys were conducted by Geo-technical Development Co. Ltd. 1953-54: Three holes, totalling 508.1 m, were drilled to test geophysical anomalies. 1960: Greenoaks drilled 303 m. 1981: Bill Miron and 487219 Ontario Ltd. optioned the Greenoaks Mine. 1982: 1,224 tons were mined by Thyssen Mining Construction Canada Ltd. for Bill Miron. 1983: Miron optioned the property to Turner Energy and Resources Ltd. Diamond-drilling, geophysics, mapping and sampling were carried out. 1985: Bill Miron held the Greenoaks Mine. 2004: Alto Ventures Ltd. acquired the property. 2007: Alto drilled 5 DDH totalling 331 m. 2008: Alto conducted trenching and sampling. 2015: Alto Ventures took 38 till samples for proccessing at Overburden Drilling Management over the Miner Lake and Greenoaks properties. 2016: Alto Ventures carried out a surface glacial till geochemistry program.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
63.390 42E13SE0063 42E13SE0063
10 42E13SW0091 42E13SW0091
2.56232 20000013950 20000013950
2.57174 20000013871 20000013871

Geology

Province: Superior

Subprovince: Wabigoon

Terrane: Eastern Wabigoon

Belt: Onaman-Tashota

Geological Age: Archean  



Geology Comments

Dec 07, 2005 (B Nelson) - The Greenoaks Mine property is underlain by intermediate to felsic metavolcanics, including andesite, dacite, rhyolite flows, tuffs, feldspar porphyry, porphyritic rhyolite and intermediate to mafic pyroclastic rocks. The Crooked Green Creek Mine and Greenoaks Mine are hosted in the same metavolcanic unit. Flow rocks appear to predominate over pyroclastic rocks. The Elmhirst Lake Stock intrudes the metavolcanics on the east portion of the property. A hybrid metavolcanic-granitoid contact zone prevents accurate identification of specific lithologies. Gold mineralization occurs in quartz veins hosted within ductile shear zones cutting metavolcanics. Zones 2, 3 and 4 were historically considered to contain low, erratic gold values over narrow widths. The No. 1 zone consists of a main quartz vein, subsidiary parallel veins (at least 3 others), fracture fillings and mineralized porphyritic host rock. The vein contains chalcopyrite, pyrrhotite and gold mineralization. The main quartz vein, which is typically blue-black (smokey), strikes 115 degrees and dips 80 degrees S to vertical. Much of the gold is present as free gold associated with the sulphides. Disseminated pyrite-pyrrhotite zones were intersected in diamond-drill core (1953) drilled to test past conductors (exact location unknown).




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Felsic lava flow-unsubdivided 1 Porphyritic Rhyolite Shear Zones Host
Vein 2 Quartz Host
Intermediate lava flow-unsubdivided 3 Andesite Near
Intermediate lava flow-unsubdivided 4 Dacite Near
Feldspar Porphyry 5 Feldspar Near
Quartz Diorite 6 Quartz Diorite Near
Diabase 7 Diabase Near

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
1ChalcopyriteEconomicOre
2GoldEconomicOre
3PyriteEconomicOre
4PyrrhotiteEconomicOre
1QuartzEconomicGangue
QuartzAlterationSilicification1UnknownDisseminated

Mineralization Comments

Dec 07, 2005 (B Nelson) - The Northern Miner (June 15, 1947) described the No. 1 zone as being 'in the form of a fork, with the handle pointing west and two prongs diverging eastward.' Channel sampling at 1.5 m intervals on the No. 1 zone indicated a zone 41.8 m long with an average width of 1.1 m, averageing 0.776 oz/ton Au. Diamond-drilling results at 15 m depths indicated the zone to be over 41.1 m in length, with an average core length of 1.6 m and grading 0.563 oz/ton Au. Grab samples taken in 1981 returned results including 0.26 oz/ton Au and 0.09 oz/ton Au.


Mar 21, 2016 (Therese Pettigrew) - Gold mineralization occurs in quartz veins hosted within ductile shear zones cutting metavolcanics. Four zones (1-4) have been identified on claim TB35563. The No. 1 zone is the main zone. Zones 2, 3, and 4 were historically considered to contain low erratic gold values over narrow widths. The No. 1 zone consists of a main quartz vein, subsidiary parallel veins (at least 3 others), fracture fillings and mineralized porphyritic host rock. The vein, contains chalcopyrite, pyrrhotite and gold mineralization. The main quartz vein, which is typically blue-black (smokey), strikes 115 degrees and dips 80 degrees S to vertical. Much of the gold is present as free gold associated with the sulphides. Disseminated pyrite-pyrrhotite zones were intersected in diamond drill core (1953) drilled to test past conductors (exact location unknown) (OFR5630). Alto’s 2007 drill program returned the following significant results: DDH GRN07-01: 12.5 g/t Au over 0.4 m from 13.2-13.6 m; DDH GRN07-04: 2.1 g/t Au over 0.5 m from 12.0-12.5 m; GRN07-04: 7.08 g/t Au over 0.8 m from 21.9-22.7 m (Alto Ventures April 3, 2007 press release).



Mineral Record Details

Classification
RankClassification            
1 Lode (Gold)
1 Vein

Site Visit Information

Date: Jan 02, 1997

Geologist: B Nelson

Notes: This property was visited by the Beardmore-Geraldton Economic Geologist November 5, 1981, in June, 1982, in August, 1982, July 20, 1983, August 4, 1983, September 27, 1983, June 5, 1984, August 7, 1984, and August 28, 1984.



Production Data
Year Tonnes Commodities Reference Comment
1982 1110 Silver 159.12 Ounces
Gold 222.77 Ounces
Copper 2703 Kilograms
OFR 5630 Produced 1224 tons at an average grade of 0.182 oz/t Au, 0.13 oz/t Ag, and 0.254% Cu.

References

Map - Sturgeon River gold area, District of Thunder Bay, Ontario

Publication Number: ARM45A Scale: 1:63,360    Date: 1998

Author: Bruce E.L., Laird H.C.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Tashota-Geraldton sheet, geological compilation series, Thunder Bay and Cochrane districts

Publication Number: M2102 Date: 1997

Author: Pye E.G., Harris F.R., Fenwick K.G., Baillie J.

Publisher Name: Ontario Dept. of Mines

Location:


Map - Elmhirst and Rickaby townships, Thunder Bay District

Publication Number: M2373 Scale: 1:31,680    Date: 1977

Author: Mackasey W.O., Wallace H.

Publisher Name: Ontario Geological Survey

Location:


Mono - Gold occurrences, prospects, and deposits of the Beardmore-Geraldton area, districts of Thunder Bay and Cochrane

Publication Number: OFR5630 Page: 218-223  Date: 1986

Author: Mason J.K., White G.D.

Publisher Name: Ontario Geological Survey

Location:


Part - The western part of the Sturgeon River area (Sturgeon R.-Beardmore section)

Publication Number: ARV45-02.002 Page: 60-117  Date: 1998

Author: Laird H.C.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of Elmhirst and Rickaby townships, District of Thunder Bay

Publication Number: R168 Date: 1978

Author: Mackasey W.O., Wallace H.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office